EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia
The Marun-Keu Complex is a Devonian subduction zone complex in the polar Ural Mountains, Russia, that preserves deep crustal processes during the Uralian Orogeny. Silica-rich fluids locally infiltrated Marun-Keu rocks at eclogite-facies conditions but only rocks adjacent to the resulting veins were...
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San Francisco State University
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ftcalifstateuniv:oai:dspace.calstate.edu:10211.3/116369 2023-05-15T18:41:28+02:00 EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia Hosseini, Pariskeh Earth & Climate Sciences 2011 http://hdl.handle.net/10211.3/116369 en_US eng San Francisco State University http://hdl.handle.net/10211.3/116369 Copyright by Pariskeh Hosseini, 2011 AS36 2011 GEOL .H67 Thesis 2011 ftcalifstateuniv 2022-04-13T11:11:15Z The Marun-Keu Complex is a Devonian subduction zone complex in the polar Ural Mountains, Russia, that preserves deep crustal processes during the Uralian Orogeny. Silica-rich fluids locally infiltrated Marun-Keu rocks at eclogite-facies conditions but only rocks adjacent to the resulting veins were eclogitized. Field and microscopic observation of the rocks from this complex show eclogitization took place across sharp, mm- to cm-scale contacts between the host rocks (amphibolite and quartzofeldspathic gneiss) and eclogite-facies rocks. A weak foliation development in Marun-Keu rocks suggests deformation may have also played a role in eclogite-facies metamorphism. This study uses electron backscatter diffraction (EBSD) to analyze crystallographic preferred orientations across these metamorphic fronts from the host rocks (amphibolite and quartzofeldspathic gneiss) to their eclogitized counterparts. Omphacite and amphibole CPOs should record eclogite- and amphibolite-facies fabric development, respectively. The EBSD analysis reveals that weak S- and S-L type fabric development in these rocks is preserved from a prograde, amphibolite-facies fabric. Any deformation during eclogitization took place in a weak stress field, in a stress field perturbed by the presence of high-pressure fluids, or fluid-induced metamorphism outlasted deformation. Fluid infiltration drove eclogitization in Marun-Keu rocks, and deformation did not play a significant role. Thesis ural mountains California State University (CSU): DSpace |
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California State University (CSU): DSpace |
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The Marun-Keu Complex is a Devonian subduction zone complex in the polar Ural Mountains, Russia, that preserves deep crustal processes during the Uralian Orogeny. Silica-rich fluids locally infiltrated Marun-Keu rocks at eclogite-facies conditions but only rocks adjacent to the resulting veins were eclogitized. Field and microscopic observation of the rocks from this complex show eclogitization took place across sharp, mm- to cm-scale contacts between the host rocks (amphibolite and quartzofeldspathic gneiss) and eclogite-facies rocks. A weak foliation development in Marun-Keu rocks suggests deformation may have also played a role in eclogite-facies metamorphism. This study uses electron backscatter diffraction (EBSD) to analyze crystallographic preferred orientations across these metamorphic fronts from the host rocks (amphibolite and quartzofeldspathic gneiss) to their eclogitized counterparts. Omphacite and amphibole CPOs should record eclogite- and amphibolite-facies fabric development, respectively. The EBSD analysis reveals that weak S- and S-L type fabric development in these rocks is preserved from a prograde, amphibolite-facies fabric. Any deformation during eclogitization took place in a weak stress field, in a stress field perturbed by the presence of high-pressure fluids, or fluid-induced metamorphism outlasted deformation. Fluid infiltration drove eclogitization in Marun-Keu rocks, and deformation did not play a significant role. |
author2 |
Earth & Climate Sciences |
format |
Thesis |
author |
Hosseini, Pariskeh |
spellingShingle |
Hosseini, Pariskeh EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
author_facet |
Hosseini, Pariskeh |
author_sort |
Hosseini, Pariskeh |
title |
EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
title_short |
EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
title_full |
EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
title_fullStr |
EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
title_full_unstemmed |
EBSD analysis of partially-eclogitized rocks from the Marun-Keu Complex, Polar Urals, Russia |
title_sort |
ebsd analysis of partially-eclogitized rocks from the marun-keu complex, polar urals, russia |
publisher |
San Francisco State University |
publishDate |
2011 |
url |
http://hdl.handle.net/10211.3/116369 |
genre |
ural mountains |
genre_facet |
ural mountains |
op_source |
AS36 2011 GEOL .H67 |
op_relation |
http://hdl.handle.net/10211.3/116369 |
op_rights |
Copyright by Pariskeh Hosseini, 2011 |
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1766230990897807360 |